文献记载的土地利用变化对平原流域地表反照率和蒸散的影响

J. Mika , Sz. Horváth , L. Makra
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引用次数: 15

摘要

农业用地系列调查在一个平原集水区的Tisza河,几乎相同的代表六个行政县。每个县通常占地34,000平方公里,其特点是管理植被的比例高(70 - 80%)。在1951-1993年期间,不同植物之间的面积覆盖变化的影响是通过应用为匈牙利指定的基于文献的综合结果来计算的。后一项研究估计了该地区种植的绝大多数植物的表面反照率值以及实际蒸散和潜在蒸散之间的比例。根据气温、降水和大气水汽压的逐月气象序列估算潜在蒸散量和土壤相对含水量。这些植物特征与地表反照率和实际蒸散发月序列的相对面积覆盖产量的乘积。此外,这些值与使用针对给定位置调整的辐射对流模式的地表-大气系统的能量平衡有关。研究了两个问题:i)在给定的能源和水收支方面是否存在单调的趋势?ii)这些变化是否可与其他外部强迫造成的影响相比较?我们的计算对这两个问题都给出了肯定的答案。
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Impact of documented land use changes on the surface albedo and evapotranspiration in a plain watershed

Agricultural land use series are investigated in a plain catchment area of the Tisza River, almost identically represented by six administrative counties. Each county, commonly covering 34,000 km2, is characterised by high percentage (70–80 %) of managed vegetation. Effects of area coverage variations between the different plants are computed for the period 1951–1993 by applying results of a literature-based syntheses, specified for Hungary. The latter studies estimate surface-albedo values and proportion between real and potential evapotranspiration for the great majority of the plants grown in the region. Potential evapotranspiration and relative soil moisture content are estimated from the monthly meteorological series of temperature, precipitation and atmospheric water vapour pressure. Product of these plant-specific characteristics and the relative area coverage yield in monthly series of surface albedo and real evapotranspiration. Furthermore, these values are related to the energy balance of the surface-atmosphere system by using a radiative-convective model adjusted for the given location. Two questions are investigated:

i) Are there monotonous trends in the given terms of the energy and water budget?

ii) Are these changes comparable to the effects caused by other external forcings?

Our computations give positive answer to both questions.

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